Persistent Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1.5–2
Several weak layers exist in the upper few feet of the snowpack. A prominent layer of surface hoar buried 1.5-2 feet deep has been responsible for a handful of skier and rider-triggered avalanches in the past few weeks. This layer is at its worst on sheltered, shady (W-N-E) slopes. Above this, you'll find a few layers of crusts, facets, and/or surface hoar that were buried in the second half of January. Today's storm will be the first good test for some of these newer weak layers.
Slides that fail on persistent weak layers are less predictable than simple wind slabs. They may break wider than you expect and may wrap around terrain features that confine wind slabs. Persistent slabs can break well above you on the slope you are skiing or riding on. Triggered wind slabs can "step-down" to these deeper weak layers, resulting in larger, more destructive avalanches.
(1/23/2023) Avalanche apparently triggered by a skier on Banner Summit. Slab depth and terrain characteristics are consistent with early January surface hoar layer. 7250', NNW. The date of this avalanche is uncertain, but likely occurred since Jan 18th. Photo taken Jan 23rd.